Meteorological Comparison of Three Cave Systems
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Pu'u Wa'awa'a Management Plan
Management Plan for the Ahupua‘a of Pu‘u Wa‘awa‘a and the Makai Lands of Pu‘u Anahulu July 15, 2003 State of Hawaii Department of Land and Natural Resources Division of Forestry and Wildlife Division of State Parks Acknowledgements In June 2002, the Pu‘u Wa‘awa‘a Advisory Council (PAC) was formed to function in a consultative capacity with Department of Land and Natural Resources (DLNR) staff involved in planning efforts for Pu‘u Wa‘awa‘a. The PAC is comprised of the following community members, who represent a wide range of expertise and interests in the various components and actions proposed in this plan: Corky Bryan Mick Castillo Dick Hoeflinger Ku‘ulei Keakealani Kepa Maly Bob Okawa Rob Pacheco Jon Sabati Michael Tomich Peter Vitousek Through a series of meetings, the PAC has reviewed several drafts of the plan and provided considerable feedback and input to DLNR staff. Many of the PAC’s suggestions have been incorporated or are now represented in this plan. The dedication, candor, and cooperation displayed by the PAC is graciously acknowledged by the DLNR. Components of this Plan relating to trails, access, ecotourism, cultural considerations, archeological resources and environmental education include modified text originally presented in a proposal by Ka ‘Ahahui o Pu‘u Wa‘awa‘a, or the “Hui”. The DLNR Management Team wishes to acknowledge and thank the Hui for permission to use these materials. Editorial Note The management objectives proposed in this management plan are not presented in a prioritized or sequential format. They are grouped by category. -
For Cody Caves Provincial Park [Electronic Resource]
Kootenay Region MANAGEMENT DIRECTION STATEMENT September 2004 for Cody Caves Ministry of Water, Land and Air Protectio Environmental Provincial Park Stewardship Division Cody Caves Provincial Park: Management Direction Statement 2004 Library and Archives Canada Cataloguing in Publication Data British Columbia. Environmental Stewardship Division. Kootenay Region. Management direction statement for Cody Caves Provincial Park [electronic resource] Cover title. At head of title: Kootenay Region. Running title: Cody Caves Provincial Park management direction statement. “September 2004” Available on the Internet. ISBN 0-7726-5356-9 1. Cody Caves Park (B.C.) 2. Provincial parks and reserves – British Columbia. 3. Ecosystem management - British Columbia – Cody Caves Park. I. British Columbia. Ministry of Water, Land and Air Protection. I. Title. II. Title: Cody Caves Provincial Park management direction statement. FC3815.C62B74 2005 333.78’30971162 C2005-960107-8 Cody Caves Provincial Park: Management Direction Statement 2004 Cody Caves Provincial Park Approvals Page Foreword This management direction statement for Cody Caves Provincial Park provides management direction until such time as a more detailed management plan may be prepared. Cody Caves Provincial Park protects an extensive cave system, and associated karst features. Approvals: Wayne Stetski Nancy Wilkin Regional Manager Assistant Deputy Minister Kootenay Region Environmental Stewardship Division Date: Date: Cody Caves Provincial Park: Management Direction Statement 2004 Table of -
The Cavernicolous Fauna of Hawaiian Lava Tubes, 1
Pacific Insects 15 (1): 139-151 20 May 1973 THE CAVERNICOLOUS FAUNA OF HAWAIIAN LAVA TUBES, 1. INTRODUCTION By Francis G. Howarth2 Abstract: The Hawaiian Islands offer great potential for evolutionary research. The discovery of specialized cavernicoles among the adaptively radiating fauna adds to that potential. About 50 lava tubes and a few other types of caves on 4 islands have been investigated. Tree roots, both living and dead, are the main energy source in the caves. Some organic material percolates into the cave through cracks associated with the roots. Cave slimes and accidentals also supply some nutrients. Lava tubes form almost exclusively in pahoehoe basalt, usually by the crusting over of lava rivers. However, the formation can be quite complex. Young basalt has numerous avenues such as vesicles, fissures, layers, and smaller tubes which allow some intercave and interlava flow dispersal of cavernicoles. In older flows these avenues are plugged by siltation or blocked or cut by erosion. The Hawaiian Islands are a string of oceanic volcanic islands stretching more than 2500 km across the mid-Pacific. The western islands are old eroded mountains which are now raised coral reefs and shoals. The eight main eastern islands total 16,667 km2 and are relatively young in geologic age. Ages range from 5+ million years for the island of Kauai to 1 million years for the largest island, Hawaii (Macdonald & Abbott, 1970). The native fauna and flora are composed of those groups which dis persed across upwards of 4000 km of open ocean or island hopped and became successfully established. -
Karst Inventory Standards and Vulnerability Assessment Procedures for British Columbia
Karst Inventory Standards and Vulnerability Assessment Procedures for British Columbia Prepared by The Karst Task Force for the Resources Inventory Committee January 2001 Version 1.0 © 2001 The Province of British Columbia Published by the Resources Inventory Committee National Library of Canada Cataloguing in Publication Data Main entry under title: Karst inventory standards and vulnerability assessment procedures for British Columbia [computer file] Available on the Internet. Issued also in printed format on demand. Includes bibliographical references: p. ISBN 0-7726-4488-8 1. Karst – British Columbia. 2. Geological surveys – British Columbia. I. Resources Inventory Committee (Canada). Karst Task Force. GB600.4.C3K37 2001 551.447 C2001-960052-6 Additional Copies of this publication can be purchased from: Government Publications Centre Phone: (250) 387-3309 or Toll free: 1-800-663-6105 Fax: (250) 387-0388 www.publications.gov.bc.ca Digital Copies are available on the Internet at: http://www.for.gov.bc.ca/ric Karst Inventory Standards Preface The Karst Inventory Standards and Vulnerability Assessment Procedures for British Columbia describes provincial standards for conducting karst inventories at various survey intensity levels, and outlines procedures for deriving karst vulnerability ratings. This document builds upon the recommendations and proposals for conducting karst inventories and vulnerability assessments described in A Preliminary Discussion of Karst Inventory Systems and Principles (KISP) for British Columbia (Research Program Working Paper 51/2000). The KISP document was widely reviewed by national and international karst experts, industry, and by staff from the Ministry of Forests and the Ministry of Environment, Lands and Parks. It is intended that these standards and procedures be implemented on an interim basis for a two-year period. -
Raw Sewage and Solid Waste Dumps in Lava Tube Caves of Hawaii Island
William R. Halliday - Raw sewarge and sold waste dumps in lave tube caves of Hawaii Island. Journal of Cave and Karst Studies, v. 65, n. 1, p. 68-75. RAW SEWAGE AND SOLID WASTE DUMPS IN LAVA TUBE CAVES OF HAWAII ISLAND WILLIAM R. HALLIDAY Hawaii Speleological Survey, 6530 Cornwall Court, Nashville, TN 37205 USA [email protected] Lava tubes on the island of Hawaii (and elsewhere) are possible subsurface point sources of contamina- tion in addition to more readily identifiable sources on the surface. Human and animal waste, and haz- ardous and toxic substances dumped into lava tube caves are subject to rapid transport during flood events, which are the dominant type of groundwater flow through Hawaiian lava tubes. Although these waste materials may not be a major source of pollution when compared with some surface sources, this potential hazard should be evaluated much as in the case of karstic floodwater conduits. This paper explores the interaction of water flow and solid waste dumps and sewage in lava tubes and lava tube caves of Hawaii Island, Hawaii - an island almost as large as the state of Connecticut (Fig. 1)-and resulting potential threats to groundwater quality. In recent years, Hawaiian cavers and speleologists have become increasingly concerned about these occurrences. Some of the solid waste dumps can be seen to contain partially empty containers of toxic and/or hazardous substances (Fig. 2), including automotive and agricultural waste. Stinking raw sewage speaks for itself (Fig. 3), and members of the Hawaii chapter of the National Speleological Society have been shown the top of a septic tank or cesspool near Keaau said to consist of an unlined segment of lava tube cave. -
Cave/Karst Management- an Integrated Ecosystems Approach
TABLE OF CONTENTS page INTRODUCTION PROVINCIAL CROWN LAND CAVE POLICY MINISTRY OF FORESTS' ROLE AND RESPONSIBILITIES COMMUNICATION AND CO-OPERATION PUBIC ACCESS CAVE/KARST MANAGEMENT- AN INTEGRATED ECOSYSTEMS APPROACH A. INVENTORY, CLASSIFICATION AND RECORDS Procedures and responsibilities B. SURFACE CONSIDERATIONS Planning and Construction for Roads and Landings Right-of-way felling, clearing and subgrade construction Pits and Quarries Fuel Storage Panning and Operations for Falling and Yarding Ground Skidding Silviculture Planning, Scarification and Burning C. SUBSURFACE CONSIDERATIONS - Visitor Use and Safety Cave User Management Guidelines D. NON-GOVERNMENT MANAGEMENT OF CAVES E. PUBLIC SAFETY AND LIABILITY F. CAVE RESCUE REFERENCES GLOSSARY OF TERMS APPENDICES INTRODUCTION British Columbia has a surface area of approximately 95 million hectares, of which 85% is crown owned forest and range land managed by the Ministry of Forests. Extensive road networks created by timber harvesting have opened the way for many recreational activities. One of these activities, which has become increasingly popular in recent years, is the sport of caving. More than 750 caves, predominantly on Vancouver Island, have been explored; and there may be hundreds, if not thousands more to be discovered. Initially recreational cavers were content to find, explore, photograph and map their finds. However, when some of the more significant caves became vandalized and or destroyed through indiscriminate resource use, individual cavers and caving groups began to advocate government participation in the management of the cave resource. These caves are a unique non-renewable resource with geological, scenic, educational, cultural, biological, hydrological, paleontological and recreation values. The management of caves [both surface and subsurface resources] is considered to be an essential component of integrated resource management. -
2018 Touring & Exploring Guide
2018 touring & exploring guide KOOTENAYROCKIES.COM 1 11 11 Red Deer 93 11 2 22 1 2 Pacific Mountain Time Time BRITISH COLUMBIA KOOTENAY Vancouver ROCKIES Calgary Kinbasket L. Portland Seattle Kalispell 93 Spokane CANADA To Jasper Montreal Minneapolis 233 km / 145 mi U S A Toronto Pacific To San Francisco Salt Lake City Chicago New York Yoho Lake Ocean Denver AtlanticEdmonton Field Louise Ban 22 294Ocean km / 183 mi C Rogers Los Angeles 2 O Pass Golden R Cochrane 23 L Houston 9 O Banff L. Minnewanka 1A U Martha C Miami M 93 Adams L. Creek Park 95 MEXICO Canyon Glacier K REGIONAL B Canmore Hot Springs Mexico1A City Calgary Mt. Revelstoke I Y To Vancouver Parson A HIGHLIGHTS 565 km / 350 mi Revelstoke Kootenay Bow Valley To Medicine M 22 HatGETTING 294 km HERE BY AIR ROAD CONDITIONS Kootenay Mount Wildland 1A Shushwap L. O Spillimacheen Assiniboine 40 Major international gateway cities 1-800-550-4997 Craigellachie Spray Kananaskis provide easy air access. Three U M Visit DriveBC.ca for real time info. Valley Country 2 Sicamous M Valley N Rockies O 22 AIR CANADA offers flights to/from Vancouver Brisco S Blanket Creek Park P Okotoks T 95 Peter & Calgary to Cranbrook and Castlegar. BORDER CROSSINGS O U ALBERTA H A REGION Lougheed Black 1-888-247-2262 Mara L. 23 U At the Canadian/US border, be sure U I Bugaboo 93 N Diamond N Galena N PACIFIC COASTAL offers scheduled flights to carry your passport or equivalent. Bay Elbow-Sheep High River Salmon Arm S 31 T to/from Vancouver into Cranbrook & Trail. -
Towards Understanding the Structure of Kaumana Cave, Hawaii
TOWARDS UNDERSTANDING THE STRUCTURE OF KAUMANA CAVE, HAWAII Stephan Kempe Inst. Applied Geosciences, Techn. Univ. Darmstadt and Hawaii Speleological Survey Schnittspahnstr. 9 Darmstadt, D-64827, Germany, [email protected] Christhild Ketz-Kempe Am Schloss Stockau 2 Dieburg, D64807, Germany, [email protected] Abstract its lower entrance at Edita Street, with bolt-marks documenting the stations. W.R. Halliday published Kaumana Cave is one of the youngest lava caves on 2003 another map, showing some of the salient cave Hawaii, formed during a few weeks at the end of the features. The cave is listed with a length of 2197 m 1880/81 Mauna Loa eruption that stopped short of according to W.R. Halliday with no vertical data given downtown Hilo. We surveyed a small section of the (Gulden, 2015). This figure represents, however, not cave above and below the Kaumana County Park the entire length of the cave. A further survey entrance in order to document the stratigraphy and conducted by D. Coons and P. Kambysis, has not yet development stages of the cave. Results show that the been published. So far, no longitudinal profile, nor roof is composed of a >10 m thick sequence of lavas cross-sections nor any detailed geological information layers, with a >3 m thick primary roof formed by five were published. to six inflationary lava sheets. The initial pyroduct had a cross-section of about 3 m2. After the placement of Kaumana Cave is part of the pyroduct that was the roof a cave developed upward by collapse of wall responsible for the advance of the 1880/1881 Mauna and roof sections. -
Journal of Cave and Karst Studies Editor Louise D
December 1998 JOURNAL OF Volume 60 Number 3 ISSN 1090-6924 CAVE AND KARST STUDIES Journal of Cave and Karst Studies Editor Louise D. Hose Volume 60 Number 3 December 1998 Environmental Studies Program Westminster College CONTENTS Fulton, MO 65251-1299 (573) 573-5303 Voice (573) 592-2217 FAX Articles [email protected] Tubular Lava Stalactites and Other Related Segregations Production Editor Kevin Allred and Carlene Allred 131 James A. Pisarowicz Wind Cave National Park Hot Springs, SD 57747 History and Status of the Moiliili Karst, Hawaii (605) 673-5582 William R. Halliday 141 [email protected] Gypsum Speleothems of Freezing Origin BOARD OF EDITORS Victor V. Korshunov and Elena V. Shavrina 146 Earth Sciences-Journal Index Ira D. Sasowsky Geochemistry of Fluorite and Related Features of the Department of Geology University of Akron Kugitangtou Ridge Caves, Turkmenistan Akron, OH 44325-4101 Vladimar Maltsev and Viktor Korshunov 151 (330) 972-5389 [email protected] The Cave-inhabiting Beetles of Cuba (Insecta: Coleoptera): Diversity, Distribution and Ecology Conservation Stewart B. Peck, Amador E. Ruiz-Baliú and George Huppert Department of Geography Gabriel F. Garcés González 156 University of Wisconsin, LaCrosse LaCrosse, WI 54601 Spatial and Temporal Variations in the Dissolved Organic [email protected] Carbon Concentrations in the Vadose Karst Waters of Marengo Cave, Indiana Life Sciences Veronica A. Toth 167 David Ashley Department of Biology Missouri Western State College The Current Status and Habitats of the Illinois Cave St. Joseph, MO 64507 Amphipod, Gammarus acherondytes Hubricht and (816) 271-4334 Mackin (Crustacea: Amphipoda) [email protected] D.W. -
Exploration of the Emesine Cave and the 1880-81 Flows of Mauna Loa
EXPLORATION of EMESINE CAVE and THE 1880-81 FLOWS OF MAUNA LOA VOLCANO by Don Coons Hawai`i Speleological Survey PO Box 7032 Ocean View Hawai`i 96737 [email protected] On May 1, 1880 an eruption of lava began in Moku`aweoweo, the summit crater of Mauna Loa on the Big Island of Hawai`i. The flow of lava is believed to have lasted for only a few days and was not easily visible at most locals on the island. In and of itself, this was not a noteworthy event. Small eruptions of this type are more or less the norm for Mauna Loa. Most residents of the island paid little attention. Volcanologists today realize that these events are important indicators of bigger things to come on Mauna Loa, the Long Mountain. On November 5, 1880 a second eruption began at an elevation of 11,000 feet along the Northeast Rift Zone of the mountain, roughly one mile above Pu`u Ula`ula. The National Park Service maintains a cabin at Red Hill along their summit trail in this area today. This second episode of the eruption sent high fountains of lava into the air as the magma found a path to the surface through narrow cracks and faults along the Rift Zone area. Though still a long ways away, this pyroclastic spectacle was clearly visible from Hilo and most of the eastern half of the island. The high fountains continued for two weeks, pumping out massive amounts of lava and creating flows down each flank of the ridgeline. -
NARACOORTE CAVES NATIONAL PARK: VISITOR FACILITY UPGRADES Deborah Carden
Journal of the Australasian Cave and Karst Management Association No. 105 December 2016 Australia Post- Print Post Approved: PP381624/02050. ISSN 1835-5374 Published Quarterly The ACKMA Journal ACKMA Inc. OFFICE BEARERS 2016-17 Official Publication of the Australasian Cave and President Karst Management Association Incorporated Dale Calnin Email: [email protected] Published quarterly in March, June, September and New Zealand Vice President December Neil Collinson Email: [email protected] The opinions expressed in the ACKMA Journal are those of the individual authors and not necessarily Australian Vice President those of ACKMA Inc. or its officers. John Brush Email: [email protected] EDITOR: Steve Bourne Executive Officer SUB EDITORS: Tony Culberg, Andy Spate Dan Cove Email: [email protected] Photos taken by the authors or editor unless Treasurer and Membership Officer otherwise acknowledged. Deborah Carden Email: [email protected] PRINTER: Hansen Print, Smith Street, Naracoorte, South Australia 5271. Ph: (08) Publications Officer and ASF Liaison Officer 87623699 Steve Bourne Email: [email protected] ACKMA Inc. is cross affiliated or otherwise Committee member associated with: Scott Melton Email: [email protected] Australian Speleological Federation, New Zealand Speleological Society, Australasian Bat Society, Committee Member The WCPA Working Group on Cave and Karst Tim Moulds Email: [email protected] Protection, Guiding Organisations Australia, Bat Conservation International, American Cave Committee Member Conservation Association, International Show Ann Augusteyn Email: [email protected] Caves Association, Cave Diving Association of Australia, The Malaysian Karst Society, The Webmaster Jenolan Caves Historical & Preservation Society Rauleigh Webb Email: [email protected] and the USA National Speleological Society Cave Conservation and Management Section Public Officer LIFE MEMBERS of ACKMA Inc. -
Evolution of Cave Living in Hawaiian Schrankia (Lepidoptera: Noctuidae) with Description of a Remarkable New Cave Species
Zoological Journal of the Linnean Society, 2009, 156, 114–139. With 11 figures Evolution of cave living in Hawaiian Schrankia (Lepidoptera: Noctuidae) with description of a remarkable new cave species MATTHEW J. MEDEIROS1*, DON DAVIS2, FRANCIS G. HOWARTH3 and ROSEMARY GILLESPIE4 1Department of Integrative Biology, University of California, 3060 Valley Life Sciences Building, Berkeley, California 94720, USA 2Department of Entomology, Smithsonian Institution, National Museum of Natural History, 10th & Constitution NW, Washington, District of Columbia 20560, USA 3Department of Natural Sciences, Bishop Museum, 1525 Bernice Street, Honolulu, Hawaii 96817, USA 4Department of Environmental Science, Policy & Management, Division of Organisms and Environment, 137 Mulford Hall MC 3114, University of California, Berkeley, California 94720, USA Received 13 March 2008; accepted for publication 12 May 2008 Although temperate cave-adapted fauna may evolve as a result of climatic change, tropical cave dwellers probably colonize caves through adaptive shifts to exploit new resources. The founding populations may have traits that make colonization of underground spaces even more likely. To investigate the process of cave adaptation and the number of times that flightlessness has evolved in a group of reportedly flightless Hawaiian cave moths, we tested the flight ability of 54 Schrankia individuals from seven caves on two islands. Several caves on one island were sampled because separate caves could have been colonized by underground connections after flightlessness had already evolved. A phylogeny based on approximately 1500 bp of mtDNA and nDNA showed that Schrankia howarthi sp. nov. invaded caves on two islands, Maui and Hawaii. Cave-adapted adults are not consistently flightless but instead are polymorphic for flight ability.